{"id":15141,"date":"2014-03-16T23:59:06","date_gmt":"2014-03-16T23:59:06","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=15141"},"modified":"2014-03-18T01:49:54","modified_gmt":"2014-03-18T01:49:54","slug":"blowing-dust-from-baja-california","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/15141","title":{"rendered":"Blowing dust from Baja California"},"content":{"rendered":"<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140316_goes15_visible_baja_blowing_dust_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-15 0.63 \u00c2\u00b5m visible channel images (click to play animation)\" alt=\"GOES-15 0.63 \u00c2\u00b5m visible channel images (click to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140316_G15_VIS_BAJA_BLDN_35.GIF\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-15 0.63 \u00c2\u00b5m visible channel images (click to play animation)<\/p><\/div>\n<p>McIDAS images of GOES-15 <em>(GOES-West)<\/em> 0.63 \u00c2\u00b5m visible channel data <em><strong>(above; click image to play animation)<\/strong><\/em> revealed large plumes of blowing dust and sand, which were moving south\/southwestward from the coast of Baja California and western Mexico on <a title=\"16 March 2014 daily weather map\" href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20140316.html\"><strong>16 March 2014<\/strong><\/a>. There were no surface observations in the immediate vicinity of the Baja California dust plume source regions, but farther to the southeast at Loreta (station identifier <a title=\"Time series of Loreta (MMLT) surface observations\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140316_MMLT_SFCMG.GIF\"><strong>MMLT<\/strong><\/a>) winds gusted to 37 knots or 43 mph at 19 UTC <em>(12 Noon local time),<\/em> and surface visibility was reduced to 3 miles. Surface winds were likely channelled by the upstream mountainous terrain to reach higher speeds near the dust plume source regions.<\/p>\n<p>A comparison of AWIPS images of Aqua MODIS 0.65 \u00c2\u00b5m visible, 1.38 \u00c2\u00b5m &#8220;cirrus detection&#8221;, 3.7 \u00c2\u00b5m shortwave IR, 11.0 \u00c2\u00b5m &#8220;IR window&#8221;, and 6.7 \u00c2\u00b5m water vapor channel data at 21:40 UTC <em><strong>(below)<\/strong><\/em> showed the following: <strong>(1)<\/strong> the dust\/sand plume could also be seen on the 1.38 \u00c2\u00b5m &#8220;cirrus detection channel&#8221; image, since this channel can be used to identify any airborne particles that are effective scatterers of light <em>(such as cirrus ice crystals, volcanic ash, haze, or dust\/sand);<\/em> <strong>(2)<\/strong> while there was no obvious dust\/sand signal on the conventional IR window channel image, the much warmer <em>(darker black)<\/em> signature on the shortwave IR image was due to reflection of incoming solar radiation off the dust\/sand particles; <strong>(3)<\/strong> on the water vapor image, an undular bore appeared to be developing near the leading edge of the dust\/sand plume. According to 1-hour interval <a title=\"MADIS\" href=\"http:\/\/madis.noaa.gov\/\"><strong>MADIS<\/strong><\/a> satellite-derived atmospheric motion vectors <em>(green wind barbs),<\/em> the plumes were moving toward the southwest at speeds as fast as 25 knots at the time.<\/p>\n<div style=\"width: 489px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140316_2140z_modis_vis_cirrus_swir_ir_wv_baja_bldn_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"Aqua MODIS 0.65 \u00c2\u00b5m visible, 1.38 \u00c2\u00b5m cirrus channel, 3.7 \u00c2\u00b5m shortwave IR, 11.0 \u00c2\u00b5m IR, and 6.7 \u00c2\u00b5m water vapor channel images\" alt=\"Aqua MODIS 0.65 \u00c2\u00b5m visible, 1.38 \u00c2\u00b5m cirrus channel, 3.7 \u00c2\u00b5m shortwave IR, 11.0 \u00c2\u00b5m IR, and 6.7 \u00c2\u00b5m water vapor channel images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140316_2140z_modis_vis_cirrus_swir_ir_wv_baja_bldn_anim.gif\" width=\"479\" height=\"349\" \/><\/a><p class=\"wp-caption-text\">Aqua MODIS 0.65 \u00c2\u00b5m visible, 1.38 \u00c2\u00b5m cirrus channel, 3.7 \u00c2\u00b5m shortwave IR, 11.0 \u00c2\u00b5m IR, and 6.7 \u00c2\u00b5m water vapor channel images<\/p><\/div>\n<p>Metop ASCAT surface scatterometer winds <em>(cyan wind barbs)<\/em> at 17:43 UTC <em><strong>(below)<\/strong><\/em> indicated that winds were northeasterly at speeds around 20 knots just off the western coast of Baja California; 18 UTC GOES-15 satellite-derived winds <em>(green wind barbs)<\/em> tracked the southwestward motion of the dust plumes at speeds of 20-31 knots.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/Scat_Winds_-_10m_20140316_1743.png\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-15 0.63 \u00c2\u00b5m visible image with GOES-15 satellite-derived winds and Metop ASCAT surface scatterometer winds\" alt=\"GOES-15 0.63 \u00c2\u00b5m visible image with GOES-15 satellite-derived winds and Metop ASCAT surface scatterometer winds\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/Scat_Winds_-_10m_20140316_1743.png\" width=\"480\" height=\"270\" \/><\/a><p class=\"wp-caption-text\">GOES-15 0.63 \u00c2\u00b5m visible image with GOES-15 satellite-derived winds and Metop ASCAT surface scatterometer winds<\/p><\/div>\n<p>A sequence of true-color Red\/Green\/Blue (RGB) images from Terra MODIS, Suomi NPP VIIRS, and Aqua MODIS viewed using the <a title=\"SSEC RealEarth web map server\" href=\"http:\/\/wms.ssec.wisc.edu\/\"><strong>SSEC RealEarth<\/strong><\/a> web map server <em><strong>(below)<\/strong><\/em> showed the southwestward progression of the tan-colored dense plumes of airborne dust\/sand from Baja California. In the initial Terra MODIS image, the source region of many of the plumes appeared to be near the <a title=\"El Vizca\u00c3\u00adno Biosphere Reserve\" href=\"http:\/\/en.wikipedia.org\/wiki\/El_Vizca%C3%ADno_Biosphere_Reserve\"><strong>El Vizca\u00c3\u00adno Biosphere Reserve<\/strong><\/a>.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140316_modis_viirs_truecolor_baja_blowing_dust_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"Terra MODIS, Suomi NPP VIIRS, and Aqua MODIS true-color RGB images\" alt=\"Terra MODIS, Suomi NPP VIIRS, and Aqua MODIS true-color RGB images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140316_modis_viirs_truecolor_baja_blowing_dust_anim.gif\" width=\"480\" height=\"294\" \/><\/a><p class=\"wp-caption-text\">Terra MODIS, Suomi NPP VIIRS, and Aqua MODIS true-color RGB images<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>McIDAS images of GOES-15 (GOES-West) 0.63 \u00c2\u00b5m visible channel data (above; click image to play animation) revealed large plumes of blowing dust and sand, which were moving south\/southwestward from the coast of Baja California and western Mexico on 16 March 2014. There were no surface observations in the immediate vicinity of the Baja California dust [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":15142,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[7,43,58,12,53,45,25,49,48],"tags":[],"class_list":["post-15141","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-air-quality","category-goes-15","category-metop","category-modis","category-real-earth","category-redgreenblue-rgb-images","category-satellite-winds","category-suomi_npp","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/15141","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/users\/18"}],"replies":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/comments?post=15141"}],"version-history":[{"count":8,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/15141\/revisions"}],"predecessor-version":[{"id":15144,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/15141\/revisions\/15144"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/15142"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=15141"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=15141"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=15141"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}